Earth, Planets and Space (Feb 2024)

The first simultaneous spectroscopic and monochromatic imaging observations of short-wavelength infrared aurora of $$\mathrm {N_{2}^{+}}$$ N 2 +  Meinel (0,0) band at 1.1 $$\mathrm {\mu }$$ μ m with incoherent scatter radar

  • Takanori Nishiyama,
  • Masato Kagitani,
  • Senri Furutachi,
  • Yuki Iwasa,
  • Yasunobu Ogawa,
  • Takuo T. Tsuda,
  • Peter Dalin,
  • Fuminori Tsuchiya,
  • Satonori Nozawa,
  • Fred Sigernes

DOI
https://doi.org/10.1186/s40623-024-01969-x
Journal volume & issue
Vol. 76, no. 1
pp. 1 – 9

Abstract

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Abstract This study presents a first simultaneous observation of $$\mathrm {N_{2}^{+}}$$ N 2 + Meinel (0,0) band (hereafter, $$\mathrm {N_{2}^{+}}$$ N 2 + (M)) aurora by cutting-edge short-wavelength infrared imaging spectrograph (NIRAS-2) and monochromatic camera (NIRAC) installed at the Kjell Henriksen Observatory (78 $$^\circ$$ ∘ N, 16 $$^\circ$$ ∘ E). On January 21 2023, $$\mathrm {N_{2}^{+}}$$ N 2 + (M) intensification that is associated with a band-shape aurora structure was observed by the NIRAS-2 and the NIRAC having temporal resolutions of 30 s and 20 s, respectively. In addition, the European incoherent scatter Svalbard Radar also observed electron density variations at the same time. Electron density measured at altitude range from 100 km 120 km shows similar variations as of $$\mathrm {N_{2}^{+}}$$ N 2 + (M) intensity, which implies that a primary source of $$\mathrm {N_{2}^{+}}$$ N 2 + (M) emissions is direct collisions of $$\mathrm {N_{2}}$$ N 2 by precipitating electrons penetrating down to around 100 km altitude (up to 10 keV). However, the observation also demonstrated moderate correlations between $$\mathrm {N_{2}^{+}}$$ N 2 + (M) intensity and electron density above 140 km, which implies that different $$\mathrm {N_{2}^{+}}$$ N 2 + (M) generation process, $$\mathrm {N_2}$$ N 2 charge exchange with $$\mathrm {O^{+}}$$ O + , may work up to near 160 km and make a non-negligible contribution to $$\mathrm {N_{2}^{+}}$$ N 2 + (M) emissions. This hypothesis would be verified with further radar observations or stereo imaging observations useful to estimate the vertical distribution of the emission layers. The $$\mathrm {N_{2}^{+}}$$ N 2 + (M) is a very promising target wavelength for aurora observation because the quality of sensors is highly expected to improve further and further. Continuous observations with our new instruments will undoubtedly provide an important information of $$\mathrm {N_{2}^{+}}$$ N 2 + (M) characteristics, for future missions of both balloon-borne and satellite-borne imaging. Graphical Abstract

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